Impacts of grain size sorting and chemical weathering on the geochemistry of Jingyuan loess in the northwestern Chinese Loess Plateau

• Published in: Journal of Asian Earth Sciences
• Main Authors: Liang, LJ (Liang, Lianji) 1,2, Sun, YB (Sun, Youbin) 1, Beets, CJ (Beets, Christiaan J.) 3, Prins, MA (Prins, Maarten A.) 3, Wu, F (Wu, Feng) 1, Vandenberghe, J (Vandenberghe, Jef) 3
• Format: Report
• Language: English
• Published: 2013
• Subjects: Chinese Loess; Elemental Geochemistry; Grain Size Sorting; Chemical Weathering; East Asian Monsoon; ice core
• Online Access: http://ir.ieecas.cn/handle/361006/9952; https://doi.org/10.1016/j.jseaes.2012.12.015

Major and trace elemental compositions of loess samples collected from the Jingyuan section in the northwestern Chinese Loess Plateau (CLP) were analyzed to investigate the potential impacts of grain size sorting and chemical weathering on the loess geochemistry and to extract appropriate geochemical indices for better evaluating the East Asian monsoon variability. Based on variations of major and trace elements in different grain size fractions, seventeen elements were classified into three types: (1) Si and Na display higher contents with the increased particle sizes; (2) Al, Fe, Mg, K, Mn, Zn, Rb, Cr, V are mainly enriched in fine size fractions; (3) Ti, Ba, Zr, P. Ca and Sr show irregular variations among different size fractions. Comparison of Al-normalized elemental ratios with Zr/Rb and Rb/Sr ratios (two commonly employed indicators for grain size sorting and pedogenic weathering) indicates that Si/Al, Zr/Al, Ti/Al variations match well with Zr/Rb and grain size results, whilst Ca/Al, Sr/Al, P/Al ratios display similar variability as that of Rb/Sr ratio. Comparison of loess based proxies (e.g., elemental ratios, magnetic susceptibility, grain size) of Jingyuan section with speleothem and ice-core records confirms that elemental ratios of high-resolution loess sequences developed in the northwestern CLP can be employed to address fluctuations of the winter monsoon-induced grain size sorting and summer monsoon-related weathering and pedogenesis at glacial-interglacial and millennial timescales.